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In each computer drawn diagram, the Miller indices of the face(s) defining the
form(s) are shown under the letters H, K, L (printed by the computer as capital
letters). The distance of this face from the centre, on an arbitrary scale, is
shown under D. The point group symmetry (shown at the top of each diagram under
the word CUBIC) then operates on the specified face (or faces) to give the
complete solid. For example, *m* 3 *m* symmetry generates all six faces of the
cube from the single face (100). For the solids thus generated from a single
face, four orthographic views are given with hidden edges omitted: a `general'
view along the [621] axis, closely similar to a standard clinographic
projection; and views along the [100], [110] and [111] directions. For each
cubic crystal viewed along the [111] direction the three-fold symmetry is
evident. There are three other equivalent three-fold axes along
[1], [1] and [1]. One
can also see immediately whether the crystal possesses a four-fold axis along
[100], a diad axis along [110], or mirror planes bisecting any of the
projections along [100], [110], and [111].

As far as possible, similarly shaped solids are placed together in the pages which follow. In some cases two different settings (`positive' and `negative') are given for the same crystal: (3 & 4, 9 & 10, 15 & 16, 19 & 20, 25 & 26); and some crystals are mirror images (enantiomorphs) of one another: (22 & 23, 27 & 28).

Table 2 lists the names of the crystal forms and table 3 shows their distribution amongst the five cubic point groups, or crystal classes.

The cube (no. 1) appears in all five columns because any one of the cubic point
group symmetries operating on the (100) plane will generate all six faces of the
cube. The rhombic dodecahedron (5) also appears five times for the same reason;
whilst the octahedron (2) appears three times, and the tetrahedron (3) twice.
210, 310 and 320 are particular examples of ; 211 and 311 of *hll* with *h* > *l* ;
and 221 is an example of *h h l* with *h* > *l* .
321 is a particular case of the general form in which all the
indices are different and non-zero. In table 3, it will be seen, for example,
that the same crystal form (15) will be generated either by 3
*m* or by 23 operating on (211).

Very often crystals exhibit faces of more than one form together. Some examples of combinations of two forms are shown here. The overall shape of a crystal is very much determined by the relative distances from the centre of the two kinds of face: one dominant form perhaps being only slightly modified by another. The drawings are still of ideal crystals, in which all faces of each form have the same size and shape. Real crystals seldom have the faces of forms so uniformly developed.

Fig. No. | Form | (Maximum) Symmetry | Name | No. of faces |

1 | 100 | m 3 m |
Cube | 6 |

2 | 111 | m 3 m |
Octahedron | 8 |

3 | 111 | Tetrahedron (positive) | 4 | |

4 | Tetrahedron (negative) | 4 | ||

5 | 110 | m 3 m |
Rhombic dodecahedron | 12 |

6 | 210 | m 3 m |
Tetrahexahedra | 24 |

7 | 310 | |||

8 | 320 | |||

9 | 210 | m 3 |
Pentagonal dodecahedra (or pyritohedra) | 12 |

10 | 120 | |||

11 | 310 | |||

12 | 320 | |||

13 | 211 | m 3 m |
Icositetrahedra (or trapezohedra) | 24 |

14 | 311 | m 3 m |
||

15 | 211 | Tristetrahedra | 12 | |

16 | ||||

17 | 311 | |||

18 | 221 | m 3 m |
Trisoctahedron | 24 |

19 | 221 | Deltoid dodecahedron (or deltohedron) | 12 | |

20 | ||||

21 | 321 | m 3 m |
Hexoctahedron | 48 |

22 | 321 | 4 3 | Pentagonal icositetrahedra (or gyroids) | |

23 | 312 | 4 3 | 24 | |

24 | 321 | Hexatetrahedron | 24 | |

25 | 321 | m 3 |
Didodecahedron (or diploid) | |

26 | 312 | m 3 |
24 | |

27 | 321 | 2 3 | Tetrahedral pentagonal dodecahedra | |

28 | 312 | 2 3 | (or tetartoids) | 12 |

(29) (30) (31) (32) (33) (34) (35) (36) (37) (38) (39) (40)

m 3 m |
4 3 | m 3 |
2 3 | ||

100 | 1 | 1 | 1 | 1 | 1 |

110 | 5 | 5 | 5 | 5 | 5 |

111 | 2 | 2 | 3 | 2 | 3 |

hk0 |
6 | 6 | 6 | 9 | 9 |

hll h > l |
13 | 13 | 15 | 13 | 15 |

hhl h > l |
18 | 18 | 19 | 18 | 19 |

h k l |
21 | 22 | 24 | 25 | 27 |

**Copyright © 1984, 1998 International Union of
Crystallography**